55-7 Effect of Conservation Agriculture On Biological Nitrogen Fixation by Soybean and Fate of 15N-Fertilizer Applied to Wheat In Semi-Arid Subtropical India.



Monday, October 17, 2011: 9:50 AM
Henry Gonzalez Convention Center, Room 214B, Concourse Level

Milkha S. Aulakh1, Joginder Manchanda1, Ashok Garg1, Gerd Dercon2 and Minh Long Nguyen2, (1)Department of Soil Science, Punjab Agricultural University, Ludhiana, India
(2)Soil and Water Management & Crop Nutrition Subprogramme, Joint FAO/IAEA Division of Nuclear Techniques in Food and Agriculture, International Atomic Energy Agency, Vienna, Austria
Nitrogen is one of the key drivers of global agricultural production. Finding ways to meet its requirement through conservation agriculture (CA), exploring biological N2 fixation (BNF) and improving plant use efficiency of fertilizer N have become extremely important tasks. Four field experiments with irrigated soybean (Glycine max L.) and wheat (Triticum aestivum L.) were conducted to estimate BNF by soybean under conventional-till (CT) and CA using 15N techniques, and to investigate the fate of 15N-fertilizer applied to succeeding wheat. Comparable amount of BNF by soybean was obtained using 15N isotope dilution and 15N natural abundance methods, suggesting that the latter method, which does not require costly 15N-enriched fertilizer, could be employed to estimate BNF by legumes. Use of sorghum as a reference plant led up to 36% lower estimation of BNF than with the use of spontaneous weeds (Eleusine aegytiacum L., Euphorbia hirta L. and , Cynodon dactylon L.), which have similar growing size, and rooting depth as the soybean. With the use of these weeds as reference plants, the irrigated soybean in the semi-arid subtropical soils could biologically fix N2 ranging from 81-125 kg ha-1 (68-85% of total N uptake), depending upon tillage and crop residue (CR) management. Significant increases in BNF by soybean were recorded where CR was retained on soil surface of CA presumably due to better activity of rhizobia because of the relatively cooler rhizosphere environment. Recovery of applied 15N in the soil-plant system at the harvest of wheat showed that 36-47% was utilized by crop, 37-49% was left in the soil profile and 5-27% was lost, which was estimated as unrecovered 15N. Utilization of 15N was significantly lower when (a) rate of fertilizer N was increased from the recommended rate of 120 kg N ha-1 to 150 kg N ha-1 in both CT and CA without CR, and (b) crop residue was incorporated in CT, or retained on the soil surface in CA. The recovery of 15N in soil profile at the harvest of wheat revealed that majority of the residual fertilizer N was present in 0-15 cm (54-61%), but downward movement of 15N below 0-15 cm soil surface layer was evident in soil profile up to 120 cm soil depth.
See more from this Division: ASA Section: Agronomic Production Systems
See more from this Session: Applied Soybean Research Community: I